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The upper Cenozoic White River tillites of...
Journal article

The upper Cenozoic White River tillites of southern Alaska: Subaerial slope and fan-delta deposits in a strike-slip setting

Abstract

The White River "tillites" crop out over 8 km2 either side of the Totschunda fault in the northern foothills of the Wrangell Mountains in southern Alaska and record glacially influenced slope and fan-delta deposition in a high-relief basin close to an active volcano between 10 and 2.7 Ma. Two measured sections, 1,200 and 450 m thick, show diamictite and conglomerates interbedded with augite andesite lavas. Facies range from massive diamictites, …

Authors

EYLES CH; EYLES N

Journal

Geological Society of America Bulletin, Vol. 101, No. 8, pp. 1091–1102

Publisher

Geological Society of America

Publication Date

August 1989

DOI

10.1130/0016-7606(1989)101<1091:tucwrt>2.3.co;2

ISSN

0016-7606